More specifically, this process is called acid dissolution.
Here's why:
* Chemical weathering involves changes in the chemical composition of rocks.
* Acid dissolution is a specific type of chemical weathering where acids react with minerals in the rock, breaking them down and dissolving them.
Common examples of acid dissolution include:
* Carbonic acid weathering: Rainwater absorbs carbon dioxide from the atmosphere, forming a weak carbonic acid. This acid can dissolve rocks like limestone and marble.
* Acid rain: Industrial pollution releases sulfur dioxide and nitrogen oxides into the atmosphere. These gases react with water vapor to form sulfuric and nitric acids, which contribute to acid rain and accelerate weathering.
* Biological weathering: Some organisms produce acids that can break down rocks, such as lichens and fungi.
